Physics for Geologists, Second edition
Physics for Geologists, Second edition
Physics for Geologists, Second edition
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Gravity 41<br />
Figure 3.9 The siphon at work. When one container is raised, it acquires poten-<br />
tial energy due to the difference in elevation, h, and this potential<br />
energy is realized by moving the water from the higher to the lower<br />
container.<br />
larger pressure in the longer arm of the tube. Clearly there is no pressure<br />
discontinuity inside the tube, and we can assume that the smallest pressure in<br />
the tube is sensibly at the crest. The pressure inside the tube at the water levels<br />
of the containers is the same on both sides - the source and the destination<br />
both being at atmospheric pressure at the surfaces of the water.<br />
The siphon can be explained in terms of the weight of fluid in the two<br />
arms of the tube, where clearly the longer arm has a greater weight of water<br />
than the shorter. The heavier side sucks the fluid from the lighter. Again,<br />
this has a limit due to the 'vacuum' created if the tube is sufficiently high.<br />
This is a valid argument <strong>for</strong> liquids, but it still comes down to energy not<br />
pressure. You will remember that the dimensions of energy are a <strong>for</strong>ce or<br />
weight times a height above an arbitrary horizontal datum, such as the table<br />
top. So the energy of the water in the higher container is greater than that<br />
of the water in the lower container, and the extra weight in the longer tube<br />
sucks the water from the shorter tube.<br />
The same principles apply to a chain passing from one bucket to another<br />
over a sheave or pulley. If you lift one bucket, the chain starts moving into<br />
the lower bucket. Energy and weight are involved, but not pressure. It does<br />
not matter how much chain is in the buckets: it is the relative energy in the<br />
chain on either side of the sheave or pulley that matters.<br />
To move anything requires energy and work.<br />
Copyright 2002 by Richard E. Chapman